Influence of the matrix of the soil-rock mixture on deformation and failure behaviors of the slope based on material point method

被引:2
|
作者
Li, Xia [1 ]
Tang, Shanyanqin [1 ]
Zheng, Yong [1 ,2 ]
Liu, Jie [3 ]
Wang, Liejian [3 ]
He, Kaiyuan [1 ]
Jiang, Tao [4 ]
机构
[1] Chongqing Jiaotong Univ, Sch River & Ocean Engn, Chongqing, Peoples R China
[2] Chongqing Municipal Educ Commiss, Key Lab Geol Hazards Mitigat Mountainous Highway &, Chongqing, Peoples R China
[3] Chongqing Water Conservancy & Elect Power Survey &, Chongqing, Peoples R China
[4] Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
soil-rock mixture; matrix; material point method; large deformation; sliding mode; FLEXIBLE MEMBRANE; DEM;
D O I
10.3389/feart.2022.997928
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this paper, the material point method (MPM) is used to explore the influence of matrix (namely soil) in the soil-rock mixture (SRM) on the stability of SRM slope. Firstly, a typical slope model is established, and a series of circular stone blocks with different sizes are generated inside the slope, then the SRM slope model is established. Next, the gravity is linearly loaded. When it is completed, the kinetic damping is applied, and the kinetic energy of the SRM slope is set to 0 to obtain the initial state of the slope. Then, the stability of the SRM slope under different soil cohesions and internal friction angles is simulated by MPM. The simulation results show that the stability of the SRM slope is more affected by cohesion than the internal friction angle. When the SRM slope enters the large deformation stage, there are both translational sliding and rotational sliding modes in the slope. The translational sliding is mainly the soil above the slope surface, and the SRM under the slope occurs rotational sliding.
引用
收藏
页数:11
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